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40Ar/39Ar Thermochronological Constraints on the Timing of Collisional Orogeny in the Mian-Lüe Collision Belt,Southern Qinling Mountains
作者姓名:LI Jinyi  WANG Zongqi  ZHAO Min
作者单位:Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037
基金项目:the former Ministry of Geology and Mineral Resources of China;8502206;
摘    要:Silurian, Devonian and Carboniferous geological bodies in the Mianxian-Lüeyang (Mian-Lüe) collisional belt (MLB) and its neighbouring areas, southern Qinling Mountains, China, show similar characteristics of having undergone deformation of two stages. The earlier one, which is inferred to be related to collisional orogeny between the Yangtze and Sino-Korean palaeocontinents based on previous geological data, is responsible for large-scale, north-verging recumbent folds and overthrusts, and associated with low greenschist facies metamorphism. 40Ar/39Ar dating of three muscovite samples taken from different localities yields plateau ages of 226.9(0.9 and 219.5(1.4 Ma and an apparent age of 194.5(3.0 Ma. Thus, the late Triassic collision between the Yangtze and Sino-Korean palaeocontinents has been constrained.

关 键 词:Qinling  Mountains  Mian-Lue  collision  belt  muscovite  40Ar/39Ar  dating  collisional  orogeny

40Ar/39Ar Thermochronological Constraints on the Timing of Collisional Orogeny in the Mian-Lüe Collision Belt,Southern Qinling Mountains
Authors:LI Jinyi  WANG Zongqi  ZHAO Min
Abstract:Silurian, Devonian and Carboniferous geological bodies in the Mianxian-Lüeyang (Mian-Lüe) collisional belt (MLB) and its neighbouring areas, southern Qinling Mountains, China, show similar characteristics of having undergone deformation of two stages. The earlier one, which is inferred to be related to collisional orogeny between the Yangtze and Sino-Korean palaeocontinents based on previous geological data, is responsible for large-scale, north-verging recumbent folds and overthrusts, and associated with low greenschist facies metamorphism. 40Ar/39Ar dating of three muscovite samples taken from different localities yields plateau ages of 226.9(0.9 and 219.5(1.4 Ma and an apparent age of 194.5(3.0 Ma. Thus, the late Triassic collision between the Yangtze and Sino-Korean palaeocontinents has been constrained.
Keywords:Qinling Mountains  Mian-Lue collision belt  muscovite  40Ar/39Ar dating  collisional orogeny
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